首页> 外文会议>International Conference on Modeling, Simulation and Applied Optimization >Assessment of the hydrological response of the watershed through a distributed physically-based modeling for extreme events: Application in the Raghay catchment (Medjerda) (Northern Tunisia)
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Assessment of the hydrological response of the watershed through a distributed physically-based modeling for extreme events: Application in the Raghay catchment (Medjerda) (Northern Tunisia)

机译:通过基于物理的分布式极端事件模型对流域的水文响应进行评估:在Raghay流域(Medjerda)中的应用(突尼斯北部)

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This research study consists on the validation of the physically and distributed hydrological model, throw the application of the ATHYS platform for hydrological modeling, for the case study of a catchment area situated in the left bank of the high valley of the Medjerda basin, the catchment area of the Raghay wadi having an area of approximately 322 km. This watershed is characterized by a very important morphological, climatic and physical variability in time and space, often presenting very important floods because of the not measured flow coming from the Algerian frontier part instead of the large difference of atitude from 165 to 1180 in the Tunisian part. The choice is fixed on six events distributed over three different seasons, recorded on the level of two pluviographic stations for an hour time-step and which control the flow in the discharge system of the catchment area. The parameters of entry of the GREEN and AMPT production function are maps having the variability of the physical parameters of the soil as well as the variation of altitude and of the directions of drainage. The advantage of this function is related on its physical base, and the theoretical possibility to estimate and optimize the parameters starting from data of grounds or “in situ” measurements. The evaluated criteria for optimization are the Nash criteria which is varying between 0.73 and 0.98 for the calibration phase, and between 0.62 and 0.75 for the validation for the three seasons, instead of the Arithmetic Mean Error for the volume and the peak flow giving very good errors for the Wintry season, good errors for the Autumnal season and medium errors for the Springer season. The results of simulations show that the selected model is well validated for the Raghay catchment than, its performance in the comprehension of the hydrological answer of a Mediterranean watershed, which provide important information for decision makers in order of protection again- t floods of the area.
机译:这项研究包括对物理和分布式水文模型的验证,并应用ATHYS平台进行水文建模,以对位于梅杰达盆地高谷左岸的集水区(集水区)为例进行研究。 Raghay旱谷的面积约322公里。该分水岭的特征是时间和空间上的形态,气候和物理变化非常重要,由于没有测量到的流量来自阿尔及利亚边境地区,而不是突尼斯的海拔高度从165变化到1180,因此经常表现出非常重要的洪水部分。该选择是固定的,分布在三个不同季节的六个事件上,记录在两个水文站的水平上,以一个小时为一个时间步长,并控制集水区排放系统中的流量。 GREEN和AMPT生产函数的输入参数是具有土壤物理参数的变化以及高度和排水方向变化的图。此功能的优点与其物理基础有关,并且与从地面数据或“原位”测量值开始估算和优化参数的理论可能性有关。优化的评估标准是纳什标准,该标准在校准阶段介于0.73和0.98之间,在三个季节的验证中介于0.62和0.75之间,而不是体积和峰值流量的算术平均误差,因此非常好。 Wintry季的错误,秋季季的错误,Springer季的中等错误。模拟结果表明,所选择的模型比其在理解地中海流域的水文答案方面的性能要好得多,在Raghay流域得到了验证,这为决策者提供了重要的信息,以保护该地区免遭洪水泛滥。 。

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